메뉴 건너뛰기




Volumn 108, Issue 1, 1998, Pages 15-32

Numerical experiments on thermal convection in a chemically stratified viscous fluid heated from below: implications for a model of lunar evolution

Author keywords

[No Author keywords available]

Indexed keywords

LUNAR EVOLUTION; THERMAL CONVECTION;

EID: 0032577191     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0031-9201(98)00096-X     Document Type: Article
Times cited : (20)

References (32)
  • 1
    • 0002735320 scopus 로고
    • Finite difference techniques for vectorized fluid dynamics calculations
    • Springer-Verlag
    • Book, D.L., 1981. Finite difference techniques for vectorized fluid dynamics calculations. Flux-corrected Transport, Chap. 6. Springer-Verlag, pp. 29-52.
    • (1981) Flux-corrected Transport, Chap. 6. , pp. 29-52
    • Book, D.L.1
  • 3
    • 0021444865 scopus 로고
    • The interaction of a subducting slab with a chemical or phase boundary
    • Christensen U.R., Yuen D.A. The interaction of a subducting slab with a chemical or phase boundary. J. Geophys. Res. 89:1984;4389-4402.
    • (1984) J. Geophys. Res. , vol.89 , pp. 4389-4402
    • Christensen, U.R.1    Yuen, D.A.2
  • 4
    • 0027396740 scopus 로고
    • Transient high-Rayleigh-number thermal convection with large viscosity variations
    • Davaille A., Jaupart C. Transient high-Rayleigh-number thermal convection with large viscosity variations. J. Fluid Mech. 253:1993;141-166.
    • (1993) J. Fluid Mech. , vol.253 , pp. 141-166
    • Davaille, A.1    Jaupart, C.2
  • 5
    • 0001220032 scopus 로고
    • Chemistry and liquidus phase relations of Apollo 15-red glasses: Implications for the lunar deep interior
    • Delano J.W. Chemistry and liquidus phase relations of Apollo 15-red glasses: implications for the lunar deep interior. Proc. Lunar Planet. Sci. Conf. 11:1980;251-288.
    • (1980) Proc. Lunar Planet. Sci. Conf. , vol.11 , pp. 251-288
    • Delano, J.W.1
  • 6
    • 0001890753 scopus 로고
    • Buoyancy driven melt segregation in the Earth's moon: I. Numerical results
    • Delano J.W. Buoyancy driven melt segregation in the Earth's moon: I. Numerical results. Proc. Lunar Planet. Sci. Conf. 20:1990;3-12.
    • (1990) Proc. Lunar Planet. Sci. Conf. , vol.20 , pp. 3-12
    • Delano, J.W.1
  • 7
    • 0010286175 scopus 로고    scopus 로고
    • Thermal convection in a volumetrically heated, infinite Prandtl number fluid with strongly temperature-dependent viscosity: Implications for planetary thermal evolution
    • submitted.
    • Grasset, O., Parmentier, E.M., 1997. Thermal convection in a volumetrically heated, infinite Prandtl number fluid with strongly temperature-dependent viscosity: implications for planetary thermal evolution. J. Geophys. Res., submitted.
    • (1997) J. Geophys. Res.
    • Grasset, O.1    Parmentier, E.M.2
  • 8
    • 85040115300 scopus 로고
    • Formation of layered structures in double-diffusive convection as applied to the geosciences
    • Hansen, U., Yuen, D.A., 1995. Formation of layered structures in double-diffusive convection as applied to the geosciences. Geophys. Monogr., Vol. 94. Am. Geophys. Union, pp. 135-149.
    • (1995) Geophys. Monogr., Vol. 94. Am. Geophys. Union , pp. 135-149
    • Hansen, U.1    Yuen, D.A.2
  • 9
    • 0029503688 scopus 로고
    • A model for the thermal and chemical evolution of the Moon's interior: Implications for the onset of mare volcanism
    • Hess P.C., Parmentier E.M. A model for the thermal and chemical evolution of the Moon's interior: implications for the onset of mare volcanism. Earth Planet. Sci. Lett. 134:1995;501-514.
    • (1995) Earth Planet. Sci. Lett. , vol.134 , pp. 501-514
    • Hess, P.C.1    Parmentier, E.M.2
  • 10
    • 0002890742 scopus 로고
    • Geophysical constraints on the lunar interior
    • In: Hartmann, W.K., Phillips, R.J., Taylor, G.J. (Eds.) Lunar and Planetary Institute, Houston
    • Hood, L.L., 1986. Geophysical constraints on the lunar interior. In: Hartmann, W.K., Phillips, R.J., Taylor, G.J. (Eds.), Origin of the Moon. Lunar and Planetary Institute, Houston, pp. 361-410.
    • (1986) Origin of the Moon , pp. 361-410
    • Hood, L.L.1
  • 11
    • 0028570982 scopus 로고
    • The role of mantle depletion and melt retention buoyancy in spreading-center segmentation
    • Jha K., Parmentier E.M., Phipps Morgan J. The role of mantle depletion and melt retention buoyancy in spreading-center segmentation. Earth Planet. Sci. Lett. 125:1994;221-234.
    • (1994) Earth Planet. Sci. Lett. , vol.125 , pp. 221-234
    • Jha, K.1    Parmentier, E.M.2    Phipps Morgan, J.3
  • 12
    • 0027430470 scopus 로고
    • Effects of mantle plumes on the growth of D″ by reaction between the core and mantle
    • Kellogg L.H., King S.D. Effects of mantle plumes on the growth of D″ by reaction between the core and mantle. Geophys. Res. Lett. 20:1993;379-382.
    • (1993) Geophys. Res. Lett. , vol.20 , pp. 379-382
    • Kellogg, L.H.1    King, S.D.2
  • 15
    • 0001856166 scopus 로고
    • Hot spots, swells, and mantle plumes
    • In: Ryan, M.P. (Ed.)
    • Olson, P., 1990. Hot spots, swells, and mantle plumes. In: Ryan, M.P. (Ed.), Magma Transport and Storage, pp. 33-51.
    • (1990) Magma Transport and Storage , pp. 33-51
    • Olson, P.1
  • 16
    • 0001363635 scopus 로고
    • Compositional and density stratification in the oceanic lithosphere - Causes and consequences
    • Oxburgh E.R., Parmentier E.M. Compositional and density stratification in the oceanic lithosphere - causes and consequences. J. Geol. Soc. London. 133:1977;343-354.
    • (1977) J. Geol. Soc. London , vol.133 , pp. 343-354
    • Oxburgh, E.R.1    Parmentier, E.M.2
  • 17
    • 0027091046 scopus 로고
    • Chemical differentiation of a convecting planetary interior: Consequences for a one-plate planet such as Venus
    • Parmentier E.M., Hess P.C. Chemical differentiation of a convecting planetary interior: consequences for a one-plate planet such as Venus. Geophys. Res. Lett. 19:1992;2015-2018.
    • (1992) Geophys. Res. Lett. , vol.19 , pp. 2015-2018
    • Parmentier, E.M.1    Hess, P.C.2
  • 19
    • 0025226481 scopus 로고
    • Permanent uplift in magmatic systems with application to the Tharsis region of Mars
    • Phillips R.J., Sleep N.H., Banerdt W.B. Permanent uplift in magmatic systems with application to the Tharsis region of Mars. J. Geophys. Res. 95:1990;5089-5100.
    • (1990) J. Geophys. Res. , vol.95 , pp. 5089-5100
    • Phillips, R.J.1    Sleep, N.H.2    Banerdt, W.B.3
  • 20
    • 0029477845 scopus 로고
    • Observational hints for a plume-fed suboceanic asthenosphere and its role in mantle convection
    • Phipps Morgan J., Morgan W.J., Zhang Y.-S., Smith W.H.F. Observational hints for a plume-fed suboceanic asthenosphere and its role in mantle convection. J. Geophys. Res. 100:1995;12753-12767.
    • (1995) J. Geophys. Res. , vol.100 , pp. 12753-12767
    • Phipps Morgan, J.1    Morgan, W.J.2    Zhang, Y.-S.3    Smith, W.H.F.4
  • 22
    • 0030434179 scopus 로고    scopus 로고
    • Hot mantle transition zone beneath Iceland and the adjacent mid-Atlantic ridge inferred from P-to-S conversions at the 410- and 660-km discontinuities
    • Shen Y., Solomon S.C., Bjarnason I.Th., Purdy G.M. Hot mantle transition zone beneath Iceland and the adjacent mid-Atlantic ridge inferred from P-to-S conversions at the 410- and 660-km discontinuities. Geophys. Res. Lett. 23:1996;3527-3530.
    • (1996) Geophys. Res. Lett. , vol.23 , pp. 3527-3530
    • Shen, Y.1    Solomon, S.C.2    Bjarnason, I.Th.3    Purdy, G.M.4
  • 23
    • 0020918558 scopus 로고
    • A simple positive definite advection transport algorithm with small implicit diffusion
    • Smolarkiewicz P.K. A simple positive definite advection transport algorithm with small implicit diffusion. Mon. Wea. Rev. 111:1983;479-486.
    • (1983) Mon. Wea. Rev. , vol.111 , pp. 479-486
    • Smolarkiewicz, P.K.1
  • 24
    • 0001097416 scopus 로고
    • A fully multidimensional positive definite advection scheme with small implicit diffusion
    • Smolarkiewicz P.K. A fully multidimensional positive definite advection scheme with small implicit diffusion. J. Comp. Phys. 54:1984;325-362.
    • (1984) J. Comp. Phys. , vol.54 , pp. 325-362
    • Smolarkiewicz, P.K.1
  • 25
    • 0001609055 scopus 로고
    • On volcanism and thermal tectonics on one-plate planets
    • Solomon S.C. On volcanism and thermal tectonics on one-plate planets. Geophys. Res. Lett. 5:1979;461-464.
    • (1979) Geophys. Res. Lett. , vol.5 , pp. 461-464
    • Solomon, S.C.1
  • 26
    • 0001026602 scopus 로고
    • Thermal expansion and thermal stress in the Moon and terrestrial planets: Clues to early thermal history
    • Solomon S.C., Chaiken J. Thermal expansion and thermal stress in the Moon and terrestrial planets: clues to early thermal history. Proc. Lunar Planet. Sci. Conf. 7:1976;3229-3243.
    • (1976) Proc. Lunar Planet. Sci. Conf. , vol.7 , pp. 3229-3243
    • Solomon, S.C.1    Chaiken, J.2
  • 27
    • 0000384710 scopus 로고
    • Magma oceanography: 1. Thermal evolution
    • Solomon S.C., Longhi J. Magma oceanography: 1. Thermal evolution. Proc. Lunar Sci. Conf. 8:1977;583-599.
    • (1977) Proc. Lunar Sci. Conf. , vol.8 , pp. 583-599
    • Solomon, S.C.1    Longhi, J.2
  • 28
    • 0015368687 scopus 로고
    • A novel finite difference formulation for differential expressions involving both first and second derivatives
    • Spalding D.B. A novel finite difference formulation for differential expressions involving both first and second derivatives. Int. J. Num. Meth. Eng. 4:1972;551-559.
    • (1972) Int. J. Num. Meth. Eng. , vol.4 , pp. 551-559
    • Spalding, D.B.1
  • 30
    • 84958430645 scopus 로고
    • The behavior of a stable salinity gradient heated from below
    • Turner J.S. The behavior of a stable salinity gradient heated from below. J. Fluid Mech. 33:1968;183-200.
    • (1968) J. Fluid Mech. , vol.33 , pp. 183-200
    • Turner, J.S.1
  • 32
    • 0000353643 scopus 로고
    • Lunar petrogenesis in a well-stirred magma ocean
    • Wood J.A. Lunar petrogenesis in a well-stirred magma ocean. Proc. Lunar Sci. Conf. 6:1975;1087-1102.
    • (1975) Proc. Lunar Sci. Conf. , vol.6 , pp. 1087-1102
    • Wood, J.A.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.